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Journal of Lipid Research, Vol. 45, 2339-2344, December 2004
Copyright © 2004 by American Society for Biochemistry and Molecular Biology


* Interdepartmental Program in Nutritional Sciences, University of Wisconsin-Madison, Madison, WI
d'Ecologie et Physiologie, Strasbourg, France
Department of Family Medicine, University of Wisconsin-Madison, Madison, WI
Published, JLR Papers in Press, September 1, 2004. DOI 10.1194/jlr.M400289-JLR200
1 To whom correspondence should be addressed. e-mail: dschoell{at}nutrisci.wisc.edu
| ABSTRACT |
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Thus, d31-palmitate can be used in outpatient settings as it eliminates the need for acetate correction and frequent sampling.
Supplementary key words substrate utilization mass spectrometry stable isotopes
| INTRODUCTION |
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40%) and the bicarbonate pool (10%), causing fat oxidation to be underestimated. To correct for this sequestration, an additional dose of [1-13C]acetate is administered. Acetate is converted to acetyl-CoA and is oxidized in the TCA cycle (4). Unfortunately, sequestration is variable and depends on the conditions under which it is measured; hence, estimation of acetate sequestration is essential (5). In addition, the use of 13C-labeled fatty acid is further constrained by the need for frequent sampling of breath and the use of a metabolic cart or respiratory chamber to quantify the flux of CO2 to calculate 13C recovery accurately. These factors increase subject burden; thus, an alternative method to quantify fat oxidation in the body would be useful. One such method for the measurement of fat oxidation is the use of deuterium-labeled fatty acids (3, 6). When oxidized, 2H-labeled fatty acid is metabolized to acetyl-CoA, releasing NADH molecules. The 2H label is released as water, in part, when NADH molecules are oxidized in the respiratory chain. Oxidation of acetyl-CoA in the TCA cycle releases the rest of the deuterium label in the form of 2H-labeled water. This 2H2O mixes with the body water and can be sampled in the urine (7). Urinary and insensible water losses are minimal (8); hence, the enrichment of label in urine can be used effectively to calculate the cumulative recovery of the label and hence the fat oxidized. Consequently, the need for measurement of CO2 and flux is also eliminated.
Deuterium-labeled palmitic acid has been validated against acetate-corrected 13C-labeled palmitic acid during rest in humans by Votruba, Zeddun, and Schoeller (6), who dosed subjects at rest with 13C- and d31-labeled palmitic acid and demonstrated that the cumulative recoveries for both tracers were highly correlated (y = 1.045x 0.47; r 2 = 0.88; P < 0.0002). More importantly, the mean difference in percentage recovery of the labels was 0.5 ± 2.8% when 13C data were corrected for acetate fixation. This method raises interesting possibilities for use under free-living conditions; however, this method has not been validated under nonresting conditions. Herein, we compared the metabolic fate of orally ingested d31-palmitate and [1-13C] palmitate during physical exercise of varying durations at moderate intensity. The objective was to ensure the validity of 2H-labeled fatty acids as an accurate tool to measure dietary fat oxidation under a range of free-living conditions.
| METHODS |
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Subjects
Healthy volunteers (six males and six females) were recruited, and their characteristics are summarized in Table 1. Two additional subjects were recruited for the measurement of natural isotope abundances and daily natural variability of isotopes in the body (body mass index = 22.8 ± 3.2 kg/m2; mean ± SD). The experimental protocol was thoroughly explained to the subjects before their recruitment into the study, and a signed informed consent was obtained from each of the subjects. The protocol was approved by the Institutional Review Board at the University of Wisconsin, Madison. Subjects completed a Physical Activity Readiness Questionnaire (9) to screen out those at risk during exercise. The physical stress test [maximum volume oxygen consumption (VO2max)] was used to determine their maximal oxygen-consuming capacities, and persons with abnormal cardiac output during this test were excluded from the study. Exclusion criteria included pregnancy; metabolic diseases such as diabetes, thyroid dysfunction, kidney malfunction, and cardiovascular diseases; and subjects who were advised by their physicians to not undertake any physical activity.
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The 24 h energy requirements of the subjects were calculated from the World Health Organization (WHO) equation (10) and were divided into 40% at dinner, 30% at breakfast, and 30% at lunch. An activity factor of 1.5 for the previous day and 1.7 for the test day were added to the WHO calculated energy expenditure. The macronutrient distribution of each standard meal consisted of 50% carbohydrates, 35% fat, and 15% protein.
On the day of the test, subjects were awakened at 6:30 AM, and a urine sample was collected at 6:45 AM. Urine and breath samples were collected at 8:00 AM to measure the natural abundance of 2H in the body water and the natural 13CO2 abundance in breath, respectively. The first visit consisted of an oral load of [1-13C]acetate at 2 mg/kg body weight and d3-acetate at 10 mg/kg body weight mixed in a liquid replacement meal (Boost high protein; Mead Johnson Nutritionals) during breakfast. The second stay consisted of an oral load of [1-13C]palmitate at 10 mg/kg body weight and d31-palmitate at 15 mg/kg body weight, mixed in the same liquid replacement meal during breakfast.
Subjects exercised at 10:00 AM for 2 h (2 hr-eEx) or 4 h at a light intensity (25% VO2max) on a cycle ergometer. Within the 4 h exercise group (n = 8), three subjects started exercise at 10:00 AM [45 min after dose; early exercise (4 hr-eEx)] and five subjects started exercise at 1:00 PM [3 h, 45 min after dose; late exercise (4 hr-lEx)].
Measurements of CO2 flux were taken for 20 min every hour. Respiratory gas exchange (RGE) was measured for 20 min every hour during the rest of the stay including at rest, during exercise, and after exercise using a Deltatrac I metabolic cart (Sensormedics). The O2 and CO2 analyzers were calibrated with a standard gas containing a 96% O2 and 4% CO2 mixture. The subjects breathed through a mouthpiece with their noses clipped to ensure complete respiratory gas monitoring. The valve is connected to a canopy system, which acts as a mixing chamber, and is exhausted into the Deltatrac system to measure the rate of oxygen consumption and carbon dioxide production. The first 5 min of measurement was excluded, and the hourly RGE was calculated assuming that the subsequent 15 min measurements per hour were representative of the whole hour.
[1-13C]palmitate oxidation rates were calculated using hourly breath samples collected when subjects blew through straws into 15 ml additive-free VacutainersTM (BD, Franklin Lakes, NJ), and d31-palmitate oxidation rates were calculated from the spot urine samples collected every hour and stored in cryogenically stable tubes (Corning, Inc.). The recovery correction factor for [1-13C] palmitate and palmitate was determined using the [1-13C]acetate and d3-acetate recovery rates.
Sample analysis
To measure the ratio of 13CO2 to 12CO2 in breath, a sample of breath was injected into a continuous-flow isotope ratio mass spectrometer (IRMS; Delta S; Finnigan MAT). The sample was injected into a continuous helium stream onto a Chromosorb-Q for separation of CO2, which is directed into the source of the IRMS. Injections were made in duplicate, and the average standard deviation was 0.3ç. Postdose enrichments within a subject were calculated using baseline predose breath samples (7).
To measure the ratio of 2H to 1H in urine, a sample (5 ml) of urine was mixed with 200 mg of carbon black to reduce impurities and was passed through a 0.45 µm filter (11). One milliliter of decolorized urine was placed in a 3 ml autosampler vial and analyzed for 2H/1H ratios using the Delta plus IRMS (Finnigan MAT). A 0.8 µl aliquot was injected into a chromium-packed quartz tube held at 850°C to reduce water to hydrogen gas. Each sample was injected three times with independent analysis. Data were corrected for H3+ and memory errors. Results were corrected to the standard mean ocean water (SMOW) scale.
Total body water was estimated from 18O enrichments in urine samples collected at baseline and 4 h after dosing with 18O-labeled water. One milliliter of decolorized urine sample was allowed to equilibrate with CO2 at 25°C for 48 h in a water bath. The 18O enrichment was measured using a continuous-flow IRMS as detailed by Schoeller and Luke (12). Total body water was calculated from the 18O data using the dilution method as described by Schoeller and van Santen (8).
Label calculations
2H and 13C label recoveries were calculated every hour for 9 h after dose. Baseline enrichment of the individual subject was subtracted from hourly recoveries to derive the increase in label recovery above baseline. Two subjects were made to follow the protocol without dosing, and the average enrichments per hour of these subjects were used to correct for natural variations in abundance of the isotopes attributable to meals and exercise. Thus, the final recovery values (
) represent individual recoveries per hour corrected for baseline abundance of individual subjects and for natural variation during the day. Rate of CO2 production (VCO2) was obtained from RGE measurements (6).
where VCO2 is measured in milliliters per minute; RSTD = 13C/12C of standard CO2; D = dose in grams; P = 13C isotope atom%; n = number of labeled atoms per molecule of tracer; MW = molecular weight of the tracer ([1-13C]acetate Na salt = 83; [1-13C]palmitic acid = 257); and isotopic enrichment above the baseline (Del) per mille (
) = (RU/ RSTD 1) x 1,000.
Breath samples were collected for 9 h after dose on both visits to correct for hourly acetate sequestration of acetate label in the TCA cycle. Deuterium recovery was calculated assuming that it is equally distributed across the total body water (TBW).
where TBW (moles) is multiplied by a factor of 1.035 to get a 2H dilution space from the TBW obtained by 18O dilution space; RSTD = 2H/1H of SMOW; D = dose in grams; P = 2H isotope atom%; n = number of labeled atoms per molecule of tracer; MW = molecular weight of the tracer (d3-acetate Na salt = 83; d31-palmitic acid = 287). The hours after dose represents the midpoint between voids for 2H recovery calculations.
Because the mean difference in body weight between visits was 0.39 ± 1.3 kg, the TBW in these subjects was assumed to be constant.
Statistical analysis
A Student's paired t-test was used to compare both tracers. Regression analysis was done to correlate the two tracers. ANOVA was used to identify the effects of exercise on the correlation of the tracers. P
0.05 was required for statistical significance. All values are presented as means ± SD. All statistical analyses were performed using STATVIEW version 5.0.1 (SAS Institute, Inc., Cary, NC).
| RESULTS |
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Acetate recovery
Cumulative 13CO2 recovery from [1-13C]acetate plateaued at
6 h after dose in all exercise groups, as shown in Fig. 1
. Cumulative [13C]acetate recoveries 3, 6, and 9 h after dose were 36.3 ± 9%, 52.6 ± 8%, and 56.8 ± 9%, respectively, indicating that most of the label was recovered at 6 h after dose in all exercise groups. 2H2O recovery from d3-acetate peaked at 45 min after dose in all three exercise groups, as shown in Fig. 1. Cumulative d3-acetate recoveries 3, 6, and 9 h after dose were 92.1 ± 8%, 90.6 ± 4%, and 88.4 ± 4%, respectively, indicating that most of the label was recovered at 3 h after dose. Compared with [1-13C]acetate, d3-acetate showed greater cumulative recovery (mean difference = 31%; P < 0.005) (Table 2). Instantaneous d3-acetate recovery was significantly higher than 13C at any time during the measurement period.
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Validation
Correlation analysis showed that cumulative d31-palmitate recovery uncorrected for acetate fixation was correlated with [1-13C]palmitate recovery group corrected for [1-13C]acetate fixation (r 2 = 0.51; y = 0.55x + 4.6; SEM = 0.19; P < 0.02) (Fig. 3)
. Because the y-intercept was not significant (P = 0.58), it was removed from the regression model (r 2 = 0.2; y = 0.96x; SEM = 0.07; P < 0.0001). When d31-palmitate recovery was corrected for acetate sequestration using group average d3-acetate recovery, the correlation r 2 was 0.56 (y = 0.74x + 4.6), and when an individual subject's d3-acetate recovery was used to correct his/her own d31-palmitate recoveries, the correlation r 2 was 0.54 (y = 0.69x + 4.9). The intercept in both of these instances was significantly different from zero (P = 0.02). The mean difference between the two tracers was lowest when uncorrected d31-palmitate recoveries were used (mean difference = 0.4 ± 3%; P = 0.64).
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| DISCUSSION |
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Although this validation was performed using stable isotope-labeled fatty acids, radioisotope-labeled fatty acids have also been used to measure dietary fatty acid oxidation under rest and exercise conditions. Romanski, Nelson, and Jensen (13) dosed their subjects with [3H]triolein and [14C]triolein along with their meal to study the trafficking of dietary fat toward oxidation or storage for 24 h after dose. Although acetate corrections for both radioisotopes were not measured, the cumulative 3H and 14C recoveries were correlated; thus, our results should apply equally well to these radioisotopes.
Carbon labeling of fatty acids appears as a natural choice for the measurement of oxidative processes, but it is subject to sequestration in the TCA, leading to reduced yield (14). Since Sidossis et al. (4) proposed the use of a correction factor for acetate sequestration in the TCA cycle intermediates, 13C-labeled fatty acids have been used for the measurement of substrate metabolism, including fatty acid oxidation rates, but their accuracy has been debated. Acetate exits the path of the labeled substrate metabolism before entry into the TCA cycle and hence can account for label sequestration occurring in the TCA cycle. The accuracy of correction for sequestration depends on the position of the label in the fatty acid and the physiological conditions under which its metabolism is measured (15).
Unlike labeled carbons, most of the 2H label from fatty acids is rapidly released as reducing power (NADH-H+ and FADH2) during ß-oxidation and then again in the TCA cycle (4). Thereafter, the 2H is oxidized to water and released into the total body water pool, which can be sampled in the urine. Because most of the NADH is formed during ß-oxidation, only
25% of the label enters the TCA cycle and only
10% of the label is expected to be sequestered (6). This estimate is supported by our data, with
88% (SEM = 1.4%) of 2H label recovered when subjects were dosed with d3-acetate. Hence, 2H-labeled fatty acids have the further advantage of not requiring an individual acetate recovery measurement and can be used independently of an acetate correction factor. An added advantage is that the time taken by the 2H label to metabolize through the intermediate pools of the body is reduced. This is shown by the more rapid appearance of 2H in urine than 13C in breath CO2 after acetate administration. This is probably attributable to the time required by 13C to pass through the TCA cycle and internal bicarbonate pools, which is eliminated when 2H label is used, because it mixes very rapidly with the body water pool (16).
Deuterium-labeled fatty acids when oxidized release the label in the body water pool, and sampling of urine measures the abundance of the isotope in the body water pool, whereas measurement of the abundance of 13CO2 in breath is an instantaneous measure of oxidation. Hence, administration of 2H label does not require the frequent measurement of VCO2 that is needed when using 13C label for the calculation of recovery. The use of hydrogen-labeled fatty acids virtually obviates the need for a controlled environment during the collection of a subject's samples. Moreover, because the tracer accumulates in body water, it reduces the potential error of missed peak oxidation with carbon labeling should the peak excretion occur between breath samples, a particularly troublesome issue with rapidly oxidized substrates such as acetate. The use of hydrogen labeling, however, requires the measurement of body water for recovery calculation, correction for water turnover for long recovery times, and is subject to dilution in the large body water pool.
Correction of 2H fatty acid oxidation measures for acetate sequestration did not yield any significant difference against uncorrected data compared with group corrected 13C fatty acid oxidation. Because the coefficient of variation for d3-acetate recovery was only 5% between individuals of all exercise groups, correction using group acetate recovery versus individual recovery did not make a discernible difference in our data. This further emphasizes that deuterium-labeled fatty acids can be used to measure dietary fat oxidation without the need for measurement of acetate correction factor.
In conclusion, we demonstrated that 2H-labeled fatty acids can be used to accurately measure the oxidation of dietary fat during exercise. Minimal sequestration of 2H label in the TCA eliminates the need for an acetate oxidation measure and hence an additional stay in the hospital. Also, compared with 13C label, 2H label can be used without the need for frequent sampling, VCO2 measurement, and restricted environment for measurements. Furthermore, high correlation between 13C-labeled fatty acids (corrected for acetate sequestration) and 2H-labeled fatty acids (uncorrected) suggests the accuracy of the measurement of fat oxidation using either method.
| ACKNOWLEDGMENTS |
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Manuscript received July 30, 2004 and in revised form August 26, 2004.
| REFERENCES |
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This article has been cited by other articles:
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A. Bergouignan, D. A. Schoeller, S. Votruba, C. Simon, and S. Blanc The acetate recovery factor to correct tracer-derived dietary fat oxidation in humans Am J Physiol Endocrinol Metab, April 1, 2008; 294(4): E645 - E653. [Abstract] [Full Text] [PDF] |
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